why is convection more important than conduction in the troposphere
Conduction and convection are two of the methods of heat transfer. Conduction, also known as diffusion is the movement of heat between objects in physical cont
act with each other. A soldering iron is a great example of transferring heat to the solder and the items being soldered by mutual physical contact. Convection is the transfer of heat via the movement of a fluid. When most fluids (liquids or gases) are heated their density decreases causing them to move relative to cooler, denser parts of the same body of fluid creating a convection current. All planetary winds are caused by convection as the Earth's rotation causes heating and expansion in some parts of the globe as the air cools in others. The other methods of heat transfer are: Radiation: a transfer of energy to or from an object via electromagnetic radiation. it's mostly what you can feel in the first the instant you turn on an electric heater, before it starts to heat the surrounding air.
Advection: moving energy from one place to another by moving a hot object. For instance used for underground hog roasts etc. where rocks are heated in a fire above ground then buried with the item to be cooked. METEOROLOGIST JEFF HABY Energy is distributed by radiation, conduction and convection. Radiation is the movement of energy in waves/particles at or near the speed of light. All objects emit radiation and the amount and wavelength of emitted radiation depends on temperature. Conduction is the movement of energy by direct contact. The classic example of this is a pan warming that is on the range. Convection is the movement of heat by the mixing that takes places in a fluid. A fluid is a gas or liquid. Convection does not take place to a significant degree in solids since the molecules are not free to move like with gas or liquids.
All three processes are important to energy transfer in the troposphere. The primary warming of the earth's surface is from the sun's radiation. Right at the surface all three distribution mechanisms take place. The sun warms the ground by radiation. The ground warms the air adjacent to the surface through conduction. Wind mixes the warmer air at the surface with cooler air aloft through convection. Certain gases can absorb radiation and warm. The classic examples of the gases that do this are ozone, carbon dioxide and water vapor. Ozone is good at absorbing UV radiation and warming. Carbon dioxide and water vapor (greenhouse gases) are good at absorbing infrared radiation and warming. At night, clouds will keep the temperatures warmer than than otherwise would be due to the absorption and thus "trapping" of infrared radiation emitted from the surface.
Conduction is a significant process immediately at the earth's surface but is not really significant above the surface since the atmosphere is composed of fluids. The temperature of the earth's surface will have a significant influence on the surface air temperature due to the conduction process. The bulk of heat energy transferred in the troposphere is done by convection. Convection does not only mean thunderstorm clouds but means any mixing of air. Air is always on the move (rising, sinking and advecting). The air mixes as it moves into the surrounding air. The winds in the troposphere and the thermals rising from the earth's surface are constantly mixing the air. Next time you are outside look for the processes of radiation, conduction and convection that are occurring in the troposphere.
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